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  • 11
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Kao, Shuh-Ji; Dai, Minhan; Wei, Kuo-Yen; Blair, N E; Lyons, William B (2008): Enhanced supply of fossil organic carbon to the Okinawa Trough since the last deglaciation. Paleoceanography, 23(2), PA2207, https://doi.org/10.1029/2007PA001440
    Publikationsdatum: 2023-06-27
    Beschreibung: Significantly older 14C ages by 2500-7900 years are found for sedimentary total organic carbon (TOC) when compared to ages of codeposited surface-dwelling foraminifera in the southern Okinawa Trough. This age discrepancy increases with rising sea level since the Last Glacial Maximum. A progressive shift in TOC d13C toward more negative values with rising sea level reflects an increasing fractional contribution of terrestrial organics (soil organics, plant debris, and/or fossil organics) to the buried organic pool. Organic matter previously stored on the East China Sea shelf during sea level lowstand and riverine material from Taiwan may be the sources that cause the d13CTOC to shift to more terrestrial values. During the Holocene when sea level is above -40 m, d13CTOC values stabilize within a narrow range (-22.3 to -22.8 per mil) while age discrepancies continue to increase and less chemically weathered sediments are deposited. The increase in age discrepancy between TOC and foraminifera in the Holocene may be due to a wetter climate that drove higher rates of physical weathering on Taiwan and greater transport rates of fossil organic C-bearing lithogenic sediment to the ocean. The climate impact on the relative delivery of fossil and nonfossil TOC in depositional settings influenced by fluvial sources should be considered in interpretations of sedimentary C isotope records.
    Schlagwort(e): Age, 14C AMS; Age, 14C calibrated; Age, dated; Age, dated standard deviation; Age, difference; Age, difference error; Calendar age; Carbon, organic, total; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Foraminifera, planktic δ13C; Formosa Strait; Giant piston corer; GPC; IMAGES VII - WEPAMA; Marion Dufresne (1995); MD012403; MD01-2403; MD122; Sample mass
    Materialart: Dataset
    Format: text/tab-separated-values, 128 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 12
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    Unbekannt
    PANGAEA
    In:  Supplement to: Kao, Shuh-Ji; Zheng, Li-Wei; Hsiao, Silver Sung-Yun (2015): Isotopic compositions and speciation of sedimentary nitrogen and carbon in the Okinawa Trough over past 30 ka. Paleoceanography, 30(10), 1233-1244, https://doi.org/10.1002/2015PA002782
    Publikationsdatum: 2023-06-27
    Beschreibung: Total organic carbon to total nitrogen ratio (C/N) and their isotopic composition (d13CTOC vs. d15NTN) are oft-applied proxies to discern terrigenous from marine sourced organics and to unravel the ancient environmental information. In high depositional Asian marginal seas, matrixes, including N-bearing minerals, dilution leads to illusive and even contradictive interpretations. We use KOH-KOBr to separate operationally defined total organic matter into oxidizable (labile) and residual fractions for content and isotope measurements. In a sediment core in the Okinawa Trough, significant amounts of carbon and nitrogen existed in the residual phase, in which the C/N ratio was ~9 resembling most documented sedimentary bulk C/N ratios in the China marginal seas. Such similarity creates a pseudo-C/N interrupting the application of bulk C/N. The residual carbon, though composition unknown, it displayed a d13C range (-22.7 to -18.9 per mil, mean -20.7 per mil) similar to black carbon (-24.0 to -22.8 per mil) in East China Sea surface sediments. After removing residual fraction, we found the temporal pattern of d13CLOC in labile fraction (LOC) was more variable but broadly agreed with the atmospheric pCO2-induced changes in marine endmember d13C. Thus, we suggested adding pCO2-induced endmember modulation into two-endmember mixing model for paleo-environment reconstruction. Meanwhile, the residual nitrogen revealed an intimate association with illite content suggesting its terrestrial origin. Additionally, d15N in residual fraction likely carried the climate imprint from land. Further studies are required to explore the controlling factors for carbon and nitrogen isotopic speciation and to retrieve the information locked in the residual fraction.
    Schlagwort(e): AGE; Carbon, organic, residual; Carbon, organic, total; DEPTH, sediment/rock; East China Sea, Pacific Ocean; Giant piston corer; GPC; IMAGES; IMAGES VII - WEPAMA; International Marine Global Change Study; Marion Dufresne (1995); MD012404; MD01-2404; MD122; Nitrogen, carbonate free fraction; Nitrogen, inorganic; δ13C, organic carbon; δ13C, residual organic carbon; δ15N, carbonate free fraction; δ15N, inorganic
    Materialart: Dataset
    Format: text/tab-separated-values, 536 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 13
    Publikationsdatum: 2023-07-10
    Schlagwort(e): Comment; Name; Protein name; Ratio; Ratio, standard deviation
    Materialart: Dataset
    Format: text/tab-separated-values, 189 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 14
    Publikationsdatum: 2024-01-27
    Schlagwort(e): DEPTH, water; DO20150330; DO20150330-track; Dongfanghong 2; LATITUDE; LONGITUDE; Nitrate; Nitrogen, organic, dissolved; Underway water sampling; UWS; δ15N, dissolved organic nitrogen; δ15N, nitrate
    Materialart: Dataset
    Format: text/tab-separated-values, 155 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 15
    Publikationsdatum: 2024-01-27
    Schlagwort(e): Ammonium; Date/Time of event; Date/Time of event 2; DO20140317; DO20140317_NWPO#1; DO20140317_NWPO#10; DO20140317_NWPO#11; DO20140317_NWPO#12; DO20140317_NWPO#13; DO20140317_NWPO#14; DO20140317_NWPO#15; DO20140317_NWPO#16; DO20140317_NWPO#17; DO20140317_NWPO#18; DO20140317_NWPO#19; DO20140317_NWPO#2; DO20140317_NWPO#20; DO20140317_NWPO#21; DO20140317_NWPO#22; DO20140317_NWPO#23; DO20140317_NWPO#24; DO20140317_NWPO#25; DO20140317_NWPO#26; DO20140317_NWPO#27; DO20140317_NWPO#28; DO20140317_NWPO#29; DO20140317_NWPO#3; DO20140317_NWPO#30; DO20140317_NWPO#31; DO20140317_NWPO#32; DO20140317_NWPO#33; DO20140317_NWPO#34; DO20140317_NWPO#35; DO20140317_NWPO#36; DO20140317_NWPO#37; DO20140317_NWPO#38; DO20140317_NWPO#39; DO20140317_NWPO#4; DO20140317_NWPO#40; DO20140317_NWPO#41; DO20140317_NWPO#42; DO20140317_NWPO#43; DO20140317_NWPO#44; DO20140317_NWPO#5; DO20140317_NWPO#6; DO20140317_NWPO#7; DO20140317_NWPO#8; DO20140317_NWPO#9; DO20150330; DO20150330_NWPO#1; DO20150330_NWPO#10; DO20150330_NWPO#11; DO20150330_NWPO#12; DO20150330_NWPO#13; DO20150330_NWPO#14; DO20150330_NWPO#15; DO20150330_NWPO#16; DO20150330_NWPO#17; DO20150330_NWPO#18; DO20150330_NWPO#19; DO20150330_NWPO#2; DO20150330_NWPO#20; DO20150330_NWPO#21; DO20150330_NWPO#22; DO20150330_NWPO#23; DO20150330_NWPO#24; DO20150330_NWPO#25; DO20150330_NWPO#26; DO20150330_NWPO#27; DO20150330_NWPO#28; DO20150330_NWPO#29; DO20150330_NWPO#3; DO20150330_NWPO#30; DO20150330_NWPO#31; DO20150330_NWPO#32; DO20150330_NWPO#33; DO20150330_NWPO#34; DO20150330_NWPO#35; DO20150330_NWPO#36; DO20150330_NWPO#37; DO20150330_NWPO#38; DO20150330_NWPO#4; DO20150330_NWPO#5; DO20150330_NWPO#6; DO20150330_NWPO#7; DO20150330_NWPO#8; DO20150330_NWPO#9; Dongfanghong 2; Event label; Latitude of event; Latitude of event 2; Longitude of event; Longitude of event 2; MULT; Multiple investigations; Nitrate; Nitrogen, total, water soluble; δ15N, nitrate; δ15N, water soluble total nitrogen
    Materialart: Dataset
    Format: text/tab-separated-values, 408 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 16
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    Unbekannt
    PANGAEA
    In:  Supplement to: Luo, Li; Kao, Shuh-Ji; Bao, Hongyan; Xiao, Huayun; Xiao, Hongwei; Yao, Xiaohong; Gao, Huiwang; Li, Jiawei; Lu, Yangyang (2018): Sources of reactive nitrogen in marine aerosol over the Northwest Pacific Ocean in spring. Atmospheric Chemistry and Physics, 18(9), 6207-6222, https://doi.org/10.5194/acp-18-6207-2018
    Publikationsdatum: 2024-01-27
    Beschreibung: Atmospheric deposition of long-range transport of anthropogenic reactive nitrogen (Nr, mainly comprised of NHx , NOy and water-soluble organic nitrogen, WSON) from continents may have profound impact on marine biogeochemistry. However, surface ocean dissolved organic nitrogen (DON) may also contribute to aerosol WSON in the overlying atmosphere. Despite the importance of off-continent dispersion and Nr interactions at the atmosphere–ocean boundary, our knowledge of the sources of various nitrogen species in the atmosphere over the open ocean remains limited due to insufficient observations. We conducted two cruises in the spring of 2014 and 2015 from the coast of China through the East China seas (ECSs, i.e. the Yellow Sea and East China Sea) to the open ocean (i.e. the north-western Pacific Ocean, NWPO). Concentrations of water-soluble total nitrogen (WSTN), NO3- and [NH4]+ , as well as the 15N of WSTN and NO3- in marine aerosol, were measured during both cruises. In the spring of 2015, we also analysed the concentrations and 15N of [NO3]- and the DON of surface seawater (SSW; at a depth of 5m) along the cruise track. Aerosol [NO3]- , [NH4]+ and WSON decreased logarithmically (1–2 orders of magnitude) with distance from the shore, reflecting strong anthropogenic emission sources of [NO3]-, [NH4]+ and WSON in China. Average aerosol [NO3]- and [NH4]+ concentrations were significantly higher in 2014 (even in the remote NWOP) than in 2015 due to the stronger wind field in 2014, underscoring the role of the Asian winter monsoon in the seaward transport of anthropogenic [NO3]- and [NH4]+ . However, the background aerosol WSON over the NWPO in 2015 (13.3±8.5 nmol/m3 was similar to that in 2014 (12.2±6.3 nmol/m3, suggesting an additional non-anthropogenic WSON source in the open ocean. Obviously, marine DON emissions should be considered in model and field assessments of net atmospheric WSON deposition in the open ocean. This study contributes information on parallel isotopic marine DON composition and aerosol Nr datasets, but more research is required to explore complex Nr sources and deposition processes in order to advance our understanding of anthropogenic influences on the marine nitrogen cycle and nitrogen exchange at land–ocean and atmosphere–ocean interfaces.
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 17
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    Unbekannt
    PANGAEA
    In:  Supplement to: Shi, Dalin; Li, Weiying; Hopkinson, Brian M; Hong, Haizheng; Li, Dongmei; Kao, Shuh-Ji; Lin, Wenfang (2015): Interactive effects of light, nitrogen source, and carbon dioxide on energy metabolism in the diatom Thalassiosira pseudonana. Limnology and Oceanography, 60(5), 1805-1822, https://doi.org/10.1002/lno.10134
    Publikationsdatum: 2024-03-15
    Beschreibung: Due to the ongoing effects of climate change, phytoplankton are likely to experience enhanced irradiance, more reduced nitrogen, and increased water acidity in the future ocean. Here, we used Thalassiosira pseudonana as a model organism to examine how phytoplankton adjust energy production and expenditure to cope with these multiple, interrelated environmental factors. Following acclimation to a matrix of irradiance, nitrogen source, and CO2 levels, the diatom's energy production and expenditures were quantified and incorporated into an energetic budget to predict how photosynthesis was affected by growth conditions. Increased light intensity and a shift from inline image to inline image led to increased energy generation, through higher rates of light capture at high light and greater investment in photosynthetic proteins when grown on inline image. Secondary energetic expenditures were adjusted modestly at different culture conditions, except that inline image utilization was systematically reduced by increasing pCO2. The subsequent changes in element stoichiometry, biochemical composition, and release of dissolved organic compounds may have important implications for marine biogeochemical cycles. The predicted effects of changing environmental conditions on photosynthesis, made using an energetic budget, were in good agreement with observations at low light, when energy is clearly limiting, but the energetic budget over-predicts the response to inline image at high light, which might be due to relief of energetic limitations and/or increased percentage of inactive photosystem II at high light. Taken together, our study demonstrates that energetic budgets offered significant insight into the response of phytoplankton energy metabolism to the changing environment and did a reasonable job predicting them.
    Schlagwort(e): Alkalinity, total; Alkalinity, total, standard deviation; Aragonite saturation state; beta-1,3 Gluan, cellular; beta-1,3 Gluan, cellular, standard deviation; Bicarbonate ion; Biomass/Abundance/Elemental composition; Bottles or small containers/Aquaria (〈20 L); Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Carbon, organic, particulate, per cell; Carbon/Nitrogen ratio; Carbon/Nitrogen ratio, standard deviation; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Carbon uptake rate; Carbon uptake rate, standard deviation; Chromista; Electron transport rate, relative; Electron transport rate, relative, standard deviation; Fatty acid content; Fatty acids, standard deviation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Gene expression (incl. proteomics); Glycolic acid, standard deviation; Glycolic acid per cell; Growth/Morphology; Growth rate; Growth rate, standard deviation; Irradiance; Laboratory experiment; Laboratory strains; Light; Macro-nutrients; Maximal electron transport rate, relative; Maximal electron transport rate, relative, standard deviation; Maximum photochemical quantum yield of photosystem II; Maximum photochemical quantum yield of photosystem II, standard deviation; mRNA copy numbers ratio; mRNA copy numbers ratio, standard deviation; mRNA gene expression, relative; mRNA gene expression, relative, standard deviation; Nitrate reductase activity; Nitrate reductase activity, standard deviation; Nitrogen uptake rate; Nitrogen uptake rate, standard deviation; Non photochemical quenching; Non photochemical quenching, standard deviation; North Pacific; OA-ICC; Ocean Acidification International Coordination Centre; Ochrophyta; Other metabolic rates; Partial pressure of carbon dioxide, standard deviation; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Particulate organic carbon content per cell, standard deviation; Particulate organic nitrogen per cell; Particulate organic nitrogen per cell, standard deviation; Pelagos; pH; pH, standard deviation; Photochemical quenching; Photochemical quenching, standard deviation; Phytoplankton; Primary production/Photosynthesis; Protein per cell; Proteins, standard deviation; PsbA expression, standard deviation; PsbA expression per cell; Registration number of species; Salinity; Single species; Species; Spectrophotometric; Temperature, water; Temperature, water, standard deviation; Thalassiosira pseudonana; Treatment; Type; Uniform resource locator/link to reference
    Materialart: Dataset
    Format: text/tab-separated-values, 552 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 18
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    Unbekannt
    PANGAEA
    In:  Supplement to: Chang, Yuan-Pin; Chen, Min-Te; Yokoyama, Yusuke; Matsuzaki, Hiroyuki; Thompson, William G; Kao, Shuh-Ji; Kawahata, Hodaka (2009): Monsoon hydrography and productivity changes in the East China Sea during the past 100,000 years: Okinawa Trough evidence (MD012404). Paleoceanography, 24(3), PA3208, https://doi.org/10.1029/2007PA001577
    Publikationsdatum: 2024-02-16
    Beschreibung: We analyzed the high-resolution foraminifer isotope records, total organic carbon (TOC), and opal content from an Okinawa Trough core MD012404 in order to estimate the monsoon hydrography and productivity changes in the East China Sea (ECS) of the tropical western Pacific over the past 100,000 years. The variability shown in the records on orbital time scales indicates that high TOC intervals coincide with the increases of boreal May-September insolation driven by precession cycles (~21 ka), implying a strong connection to the variations in monsoons. We also observed possibly nearly synchronous, millennial-scale changes of the ECS surface hydrography (mainly driven by salinity changes but also by temperature effects) and productivity coincident with monsoon events in the Hulu/Dongge stalagmite isotope records. We found that increased freshening and high productivity correlate with high monsoon intensity in interstadials. This study suggests that the millennial-scale changes in monsoon hydrography and productivity in the ECS are remarkable and persistent features over the past 100,000 years.
    Schlagwort(e): Age, 14C AMS; Age, dated; Age, dated material; Age, dated standard deviation; Calendar age; DEPTH, sediment/rock; East China Sea, Pacific Ocean; Giant piston corer; GPC; IMAGES VII - WEPAMA; Isotopic event; Marion Dufresne (1995); MD012404; MD01-2404; MD122
    Materialart: Dataset
    Format: text/tab-separated-values, 90 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 19
    Publikationsdatum: 2022-05-25
    Beschreibung: Author Posting. © American Geophysical Union, 2009. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 24 (2009): PA3208, doi:10.1029/2007PA001577.
    Beschreibung: We analyzed the high-resolution foraminifer isotope records, total organic carbon (TOC), and opal content from an Okinawa Trough core MD012404 in order to estimate the monsoon hydrography and productivity changes in the East China Sea (ECS) of the tropical western Pacific over the past 100,000 years. The variability shown in the records on orbital time scales indicates that high TOC intervals coincide with the increases of boreal May–September insolation driven by precession cycles (∼21 ka), implying a strong connection to the variations in monsoons. We also observed possibly nearly synchronous, millennial-scale changes of the ECS surface hydrography (mainly driven by salinity changes but also by temperature effects) and productivity coincident with monsoon events in the Hulu/Dongge stalagmite isotope records. We found that increased freshening and high productivity correlate with high monsoon intensity in interstadials. This study suggests that the millennial-scale changes in monsoon hydrography and productivity in the ECS are remarkable and persistent features over the past 100,000 years.
    Beschreibung: Y.Y.’s work was partly supported by Global Environmental Research Fund (RF-081) and JSPS Kakenhi (21674003).
    Schlagwort(e): Monsoon ; Productivity ; Precipitation ; Precession ; Okinawa Trough ; East China Sea
    Repository-Name: Woods Hole Open Access Server
    Materialart: Article
    Format: application/pdf
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 20
    Publikationsdatum: 2022-05-25
    Beschreibung: Author Posting. © American Geophysical Union, 2010. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 37 (2010): L21702, doi:10.1029/2010GL044893.
    Beschreibung: The western tropical Pacific gives birth to 23 tropical cyclones annually, bringing torrential rainfall to mountainous islands across Oceania resulting in a global sediment production hotspot, in which many rivers have great hyperpycnal potential. By using a temperature (T) and salinity (S) profiler, we observed anomalously warm, low salinity turbid water at 3000–3700 m depths in seas ∼180 km off southwestern Taiwan immediately after Typhoon Morakot in 2009. This 250m-thick bottom-hugging water occupies ∼2400 km2, and contains 0.15% freshwater, suggesting a remarkably high fraction (6–10%) of event rainfall from southwestern Taiwan. These characteristics indicate the turbid water originated from shallow coastal waters via hyperpycnal flow. Apparently, sediment produced from the land during tropical cyclones open an “express gate” to convey heat and freshwater vertically to the deep ocean basin subsequently warming the deep water from the bottom up.
    Beschreibung: Funded by China (973 Program, 2009CB421200 and the program of Introducing Talents of Discipline to Universities, B07034) and Taiwan (NSC 98‐2116‐M‐001‐005; Academia Sinica Thematic Program AFOBi).
    Schlagwort(e): Cycloen ; Hyperpycnal flow ; Typhoon Morakot ; Taiwan ; Oceania
    Repository-Name: Woods Hole Open Access Server
    Materialart: Article
    Format: application/pdf
    Standort Signatur Einschränkungen Verfügbarkeit
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